2017
DOI: 10.1002/ecs2.1656
|View full text |Cite
|
Sign up to set email alerts
|

Effects of grazing on ecosystem structure and function of alpine grasslands in Qinghai–Tibetan Plateau: a synthesis

Abstract: 1656Abstract. Humans have grazed on the Qinghai-Tibetan Plateau (QTP) for many thousands of years. In recent decades, the intensity of grazing has increased and several new management strategies have been put into place to address the resulting changes in rangeland condition. Effective management of grazing activities in this region requires understanding the impact of livestock grazing across the diverse array of alpine grassland ecosystems present in the QTP, but recent studies have identified a number of cr… Show more

Help me understand this report

Search citation statements

Order By: Relevance

Paper Sections

Select...
3
1
1

Citation Types

20
109
3
1

Year Published

2017
2017
2019
2019

Publication Types

Select...
7

Relationship

0
7

Authors

Journals

citations
Cited by 180 publications
(139 citation statements)
references
References 98 publications
20
109
3
1
Order By: Relevance
“…() found that soil C loss is primarily attributed to the reduced heavy fraction organic carbon. An increase in soil pH is also expected under conditions of intensified trampling, as it causes topsoil removal and lowers the soil surface towards the more alkaline subsoil (Evans et al ., ). With continuous (nonrotational) grazing under the SMP, plants can be smaller, resulting in less plant cover and biomass, as confirmed in Maqu by our previous studies (Cao et al ., , ), which in turn leads to less C inputs to form SOC (Wang et al ., ; Lu et al ., ). One possible reason for this is that an important portion of the photosynthetic tissue is consumed and subsequent respiration of assimilated C by herbivores increases C outputs from the ecosystem and reduces C available for the formation of SOC (Klumpp et al ., ; Piñeiro et al ., ).…”
Section: Discussionmentioning
confidence: 97%
“…() found that soil C loss is primarily attributed to the reduced heavy fraction organic carbon. An increase in soil pH is also expected under conditions of intensified trampling, as it causes topsoil removal and lowers the soil surface towards the more alkaline subsoil (Evans et al ., ). With continuous (nonrotational) grazing under the SMP, plants can be smaller, resulting in less plant cover and biomass, as confirmed in Maqu by our previous studies (Cao et al ., , ), which in turn leads to less C inputs to form SOC (Wang et al ., ; Lu et al ., ). One possible reason for this is that an important portion of the photosynthetic tissue is consumed and subsequent respiration of assimilated C by herbivores increases C outputs from the ecosystem and reduces C available for the formation of SOC (Klumpp et al ., ; Piñeiro et al ., ).…”
Section: Discussionmentioning
confidence: 97%
“…Globally, grazing patterns are rapidly changing. In some regions such as European mountain ranges, the cessation of grazing is typical, while in most lowland regions of Australia, Africa, Asia, South America, and the Mediterranean, overgrazing has become typical (Abu Hammad & Tumeizi, ; Evans et al., ; Lu et al., ; Rowntree, Duma, Kakembo, & Thornes, ; Vetter & Bond, ). In several regions within the vast Palaearctic steppe zone, which stretches from Eastern Europe to Northeast China, overgrazing, alongside land conversion, became the most important driver of declining grassland biodiversity in the last few decades (Wesche et al., ).…”
Section: Introductionmentioning
confidence: 99%
“…A study by Lu et al. () of many paired grazed and un‐grazed grassland sites on the QTP suggested plant species richness declined in the absence of stocking whereas soil carbon, nitrogen, and microbial biomass increased.…”
Section: Introductionmentioning
confidence: 99%
“…It is possible that differences in perceived degradation arose from a combination of factors such as the cooccurrence of drought and grazing rather than stocking rate per se. A study by Lu et al (2017) of many paired grazed and un-grazed grassland sites on the QTP suggested plant species richness declined in the absence of stocking whereas soil carbon, nitrogen, and microbial biomass increased.…”
Section: Introductionmentioning
confidence: 99%